Official Series Description


Lab Data Summary

Aggregate lab data for the OKAN soil series. This aggregation is based on all pedons with a current taxon name of OKAN, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to OKAN were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the OKAN soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the OKAN series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the OKAN series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the OKAN series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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There are insufficient data to create the 3D mountains figure.

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Competing Series

Soil series competing with OKAN share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the OKAN series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the OKAN series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with OKAN, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

No block diagrams are available.

Map Units

Map units containing OKAN as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Eastwell-Wintermute-Okan association63117249478415j1trnv76619941:24000
Shabliss-Okan-Eastwell association35116139478302j1q3nv76619941:24000
Automal-Okan-Wintermute association50315609478364j1s3nv76619941:24000
Linoyer-Okan association37111649478311j1qdnv76619941:24000
Zafod-Automal-Okan association10708975478578j200nv76619941:24000
Shabliss-Pyrat-Okan association2828334478286j1plnv76619941:24000
Okan-Automal association11208018478584j206nv76619941:24000
Wesfil-Wintermute-Okan association927112478199j1lsnv76619941:24000
Pyrat-Okan-Eastwell association10017019478555j1z8nv76619941:24000
Pharo-Izar-Okan association5016701478362j1s1nv76619941:24000
Mazuma-Zerk-Okan association8015584478467j1wfnv76619941:24000
Shabliss-Okan association3555578478306j1q7nv76619941:24000
Okan-Eastwell-Blimo association10205486478566j1zmnv76619941:24000
Palinor-Hundraw-Okan association4245247478331j1r1nv76619941:24000
Heist-Okan-Zerk association3745100478314j1qhnv76619941:24000
Palinor-Wintermute-Okan association8504332478496j1xcnv76619941:24000
Okan-Pyrat association9324158478533j1yknv76619941:24000
Wintermute-Linoyer-Okan association1744044478240j1n3nv76619941:24000
Okan-Automal-Hundraw association4603595478345j1rhnv76619941:24000
Izar-Hundraw-Okan association2523530478275j1p7nv76619941:24000
Eastwell-Hundraw-Okan association6363216478420j1txnv76619941:24000
Okan-Katelana association10233056478569j1zqnv76619941:24000
Palinor-Zimbob-Okan association4222972478329j1qznv76619941:24000
Okan-Toano-Loray association9302387478531j1yhnv76619941:24000
Threesee-Linoyer-Okan association14111527478635j21vnv76619941:24000

Map of Series Extent

Approximate geographic distribution of the OKAN soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .